A fact from Moine Supergroup appeared on Wikipedia's Main Page in the Did you know column on 16 September 2009 (check views). The text of the entry was as follows:
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This article is impacted by the work of Krabbendam and co-workers in 2021 2022. Taking this into account will require a rewrite, which I may get around to at some point. Mikenorton (talk) 15:42, 15 May 2024 (UTC)[reply]
Goodness, (interesting article btw) I shall mourn the passing of the Moine into history, this and the Torridonian having been backdrops to all considerations of Northwest Highland landscapes throughout my geological life. That said, just as with similar developments elsewhere (the Old Red has been substantially revised here in the Anglo-Welsh basin), they'll remain with us through maps and references for decades to come, so will still need to be referred to. Good luck with the re-write! Geopersona (talk) 16:02, 15 May 2024 (UTC)[reply]
It's fascinating and hard to fault on what I know, although I'm not sure that we can regard it as fully accepted yet. When I created the Moine article in 2009 and rewrote the Torridonian one (with help) in 2010, it all seemed so simple but that's the way with geology. Oddly enough, it was only last year that I first saw the Moine and the Torridonian in the field (apart from some Moinian stuff in Caithness, Orkney and Shetland when I was working on the Devonian in those parts). I've still never seen the Moine Thrust. Mikenorton (talk) 16:32, 15 May 2024 (UTC)[reply]
